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purple, green and yellow. Its lustre is generally vitreous. Crystals are cubic, octahedral or dodecahedral with a cleavage parallel to the octahedral. Hardness is 4. Fluorite occurs as a gangue mineral in medium to high temperature hydrothermal veins associated with lead, zinc and silver sulphides. It can also occur in pegmatites and as an accessory mineral in the cavities of felsic intrusives. World class deposits can be found in Canada (Ontario), USA (Kentucky), England (Derbyshire: Blue John Caves) and Mexico. and plastics industries. Very pure crystals can be used in spectrographic prisms.
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